Cited by 185Planetary Science and ExplorationGeochemistry and Elemental AnalysisAstro and Planetary Science

Rates and mechanisms of chemical weathering of ferromagnesian silicate minerals on Mars

Burns, Roger G·1993·Geochimica et Cosmochimica Acta

Integrity signals

Registry

Crossref · 10.1016/0016-7037(93)90182-v

Cites

6 of 6 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • Ferromagnesian silicates, typical of Martian igneous rocks, are dissolved by acidic water to produce cations including Fe2+, Mg2+, Ca2+, K+, Na+, and silica in roughly stoichiometric proportion to the mineral composition under low-oxygen conditions.

    “Ferromagnesian silicates, typical of Martian igneous rocks, are dissolved by such acidic water to produce curious including Fe 2+, Mg •+, Ca 2+, K +, Na +, and silica in roughly stoichiometric proportion to the mineral composition under low-oxygen conditions, according to laboratory experiments [Murphy and Helgeson, 1989; Burns, 1993].”
  • Fe2+ and Mg2+ behave very similarly during anoxic weathering of mafic rock and dissolve in proportion to their stoichiometry.

    “We set the molal concentration of Fe 2+ relative to that of Mg a+ because these two curious behave very similarly during anoxic weathering of mafic rock and dissolve in proportion to their stoichiometry [e.g., Burns, 1993].”

Cites

Flagged first, then by citations

Cited by

Sorted by citations

Authors
Burns, R. G.
Affiliations
Massachusetts Institute of Technology (US)
Corresponding author
Burns, Roger G
Venue
Geochimica et Cosmochimica Acta
Publisher
Elsevier BV
Published
1993-10
Volume
57
Issue
19
Pages
4555-4574
ISSN
0016-7037 (ISSN-L)
OpenAlex
W2083317216
Cited by
185
References
6
Citations by year
2026: 2 · 2025: 10 · 2024: 5 · 2023: 2 · 2022: 9 · 2021: 6 · 2020: 3 · 2019: 3 · 2018: 3 · 2017: 9 · 2016: 7 · 2015: 3 · 2014: 5 · 2013: 9 · 2012: 7
FWCI
3.00
Type
journal article
Language
en
Open access
closed
Locations
Geochimica et Cosmochimica Acta (publishedVersion)
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Planetary Science and Exploration
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
Keywords
chemical weathering, Mars, ferromagnesian silicates, olivine, pyroxene, oxidative weathering, ferrolysis, iron oxidation, iron dissolution, Martian meteorites, Martian basalts, saponite, ferric oxide, hydrolysis, aqueous alteration, Mars climate history

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review